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A Synthesis of Progress and Uncertainties in Attributing the Sources of Mercury in Deposition

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TLDR
It is agreed that the uncertainty is strongly dependent upon scale and that the question as stated is answerable with greater confidence both very near and very far from major point sources, assuming that the “global pool” is a recognizable “source.”
Abstract
A panel of international experts was convened in Madison, Wisconsin, in 2005, as part of the 8th International Conference on Mercury as a Global Pollutant. Our charge was to address the state of science pertinent to source attribution, specifically our key question was: "For a given location, can we ascertain with confidence the relative contributions of local, regional, and global sources, and of natural versus anthropogenic emissions to mercury deposition?" The panel synthesized new research pertinent to this question published over the past decade, with emphasis on four major research topics: long-term anthropogenic change, current emission and deposition trends, chemical transformations and cycling, and modeling and uncertainty. Within each topic, the panel drew a series of conclusions, which are presented in this paper. These conclusions led us to concur that the answer to our question is a "qualified yes," with the qualification being dependent upon the level of uncertainty one is willing to accept. We agreed that the uncertainty is strongly dependent upon scale and that our question as stated is answerable with greater confidence both very near and very far from major point sources, assuming that the "global pool" is a recognizable "source." Many regions of interest from an ecosystem-exposure standpoint lie in between, where source attribution carries the greatest degree of uncertainty.

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Citations
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Journal ArticleDOI

Mercury as a Global Pollutant: Sources, Pathways, and Effects

TL;DR: Understanding of sources, atmosphere-land-ocean Hg dynamics and health effects are synthesized, and integration of Hg science with national and international policy efforts is needed to target efforts and evaluate efficacy.
Journal ArticleDOI

Global Biogeochemical Cycling of Mercury: A Review

TL;DR: In this paper, the authors studied uncertainty in the global biogeochemical cycle of mercury, including oxidation processes in the atmosphere, land atmosphere and ocean-atmosphere cycling.
Journal ArticleDOI

Mechanisms Regulating Mercury Bioavailability for Methylating Microorganisms in the Aquatic Environment: A Critical Review

TL;DR: This Review evaluates the current state of knowledge regarding the mechanisms regulating microbial mercury methylation, including the speciation of mercury in environments where methylation occurs and the processes that control mercury bioavailability to these organisms.
References
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Journal ArticleDOI

Modern and historic atmospheric mercury fluxes in both hemispheres: Global and regional mercury cycling implications

TL;DR: In this article, the atmospheric deposition of mercury (Hg) over the last 800-1000 years in both hemispheres was reconstructed using two different natural archiving media from remote locations.
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Global circulation of atmospheric mercury: a modelling study

TL;DR: In this paper, the authors present a comprehensive atmospheric global and regional mercury model and its capability in describing the atmospheric cycling of mercury, which can be used to understand the role of meteorology in mercury cycling (atmospheric pathways), the inter-annual variability of mercury and can be evaluated against observations on global scales.
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A kinetic study of the gas-phase reaction between the hydroxyl radical and atomic mercury

TL;DR: In this paper, the kinetics of the gas phase reaction between atomic mercury and hydroxyl radical has been determined at room temperature and atmospheric pressure of air by relative rate technique, and the rate coefficient obtained was k(Hg 0 + · OH )=(8.7±2.8)×10 −14 cm 3 s −1 leading to natural lifetimes of mercury at global mean conditions of 4-7 month due to this reaction.
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Modern and historic atmospheric mercury fluxes in northern Alaska: Global sources and Arctic depletion

TL;DR: Recovering from lake-sediment archives atmospheric Hg deposition to Arctic Alaska over the last several centuries and constrain a contemporary lake/watershed mass-balance with real-time measurement of Hg fluxes in rainfall, runoff, and evasion indicates anthropogenic Hg impact in the Arctic is of similar magnitude to that at temperate latitudes.
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The role of mercury redox reactions in snow on snow-to-air mercury transfer.

TL;DR: The snow-to-air Hg transfer observed in this study suggests that the massive Hg deposition events observed in springtime in northern environments may have less impact than previously anticipated, since once deposited, Hg could be rapidly reduced and re-emitted.
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